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”ŽŽm

•½¬25”N3ŒŽC—¹(•½¬24”N“x)

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¬¼ Œ’‰îWaveform inversion for localized 3-D seismic velocity structure in the lowermost mantle beneath the Western Pacific
íî“c —m•½Investigation of slip parameters and fault slip behavior in the shallow part of subduction zone on the basis of vitrinite reflectance

•½¬22”N3ŒŽC—¹(•½¬21”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
ã–Ø Œ«‘¾Origin of arc magmas in the Sengan region, Northeastern Japan and Thermodynamic modeling of mantle melting
•yŽm ‰„ÍA methodology for inversion of seismic waveforms for elastic and anelastic structure and its preliminary application to the mantle transition zone benath the Northwestern Pacific

•½¬21”N3ŒŽC—¹(•½¬20”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
Tae-Ho PARKChronological and Petrological Study of Cretaceous to Paleogene Granitic Rocks, South Korea
‰ª“c ^‰îCrustal extension and shortening in the back-arc region of Northeast Japan
òŽR “O–çIncremental melting process and thermal evolution of an upwelling mantle: constraints from back arc volcanisms in the eastern margin of the Eurasian Plate
“ào ’•FObservational study on the self-similarity of earthquake rupture growth in Parkfield area
²“¡ —FŽqSiO2 ƒKƒ‰ƒX‚Ì–§“x‚Æ\‘¢‚Ì’´‚ˆ³‰º‚»‚Ìꑪ’è
–ì“c Žé”üGPS Data Inversion to Estimate 3-D Elastic/Inelastic Strain Fields in Island-Arc Crust
ŽRŒû ”ò’¹Linkage between faulting, fluid flow and earthquake generation in seismogenic subduction zones

•½¬20”N9ŒŽC—¹(•½¬20”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
Ž­‘q —m‰îNumerical Simulation with a Finite Element Method for the Development of Mechanical and Thermal Structure in Subduction Zones

•½¬20”N3ŒŽC—¹(•½¬19”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
‰¬’à ’BWater content of the upper mantle benearth island arcs and its tectonic implications: Petrologic study of Aogashima Volcano, Izu Arc, Japan
—é–Ø ÊŽqNew deformation indicator for peridotites in the upper mantle: Experimental study on diffusion in chromite spinel
ì’[ ŒP‘ãQuantitative examinations of mass transfer by pressure solution and fluid flow in natural deformation zones

•½¬19”N3ŒŽC—¹(•½¬18”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
•½—Ñ LNDevelopment of a finite-difference scheme using optimally accurate operators for computation of synthetic seismograms in heterogeneous media and its applicability to geophysical exploration

•½¬18”N9ŒŽC—¹(•½¬18”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
‹´ŠÔ º“¿Internal Deformation Fields due to a Moment Tensor in an Elastic-Viscoelastic Layered Half-Space: Application to Tectonics of Back-Arc Basins
–k‘º —LvA fate of sediments in subduction zone
ՠԼ mӟGeochemical variations of volcanic rocks in Central Japan: Implication for the fluid processes in subduction zone with the double subducting plates

•½¬18”N3ŒŽC—¹(•½¬17”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
Ž›ì ŽõŽqAbsolute Strength of the San Andreas Fault Inferred from Tectonic Loading Simulation and CMT Data Inversion
‰Í‡ Œ¤ŽuMethods for waveform inversion for localized seismic structure

•½¬16”N3ŒŽC—¹(•½¬15”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
“c—Í ³D‘æŽl‹IŒãŠú‚É‚¨‚¯‚é“Œ–k“ú–{ŒÊ‚Ì’nŠk•Ï“®pdf
Žu‘º —æŽq”Âóƒ}ƒOƒ}—­‚Ü‚è‚Ì”M‰»Šwi‰»‰ß’öF”[¹•z–¦ŠÑ“üŠâ‘Ì‚©‚ç‚̧–ñpdf

CŽm

•½¬25”N3ŒŽC—¹i•½¬24”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
ŒÜ\—’ ŒõŽk‹‘å’nk‚ÌŽ©—RU“®‚ð—p‚¢‚½‚ä‚Á‚­‚è‚Æ‚µ‚½‚·‚ׂè‚ÌŒŸoƒQƒ‰[ ƒƒo[ƒg

•½¬24”N3ŒŽC—¹i•½¬23”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
ŒIŒ´ ‹`Ž¡Statistical analysis of seismicity by discretized triggering model i—£ŽU“IƒgƒŠƒKƒŠƒ“ƒOƒ‚ƒfƒ‹‚É‚æ‚é’nkŠˆ“®‚Ì“Œv“I‰ðÍjˆäo “N
‰––¡ —I–çÆ«/‘Y«‘JˆÚ—̈æ‚É‚¨‚¯‚é™’’f‘Ñ‚Ì”ñ‘ÎÌ«‚ɂ‚¢‚Ä‚ÌlŽ@“c’† GŽÀ
¼ŽR Œ’ŽuAnalysis of Size, Geometry, and Motion of PlatesiƒvƒŒ[ƒg‚̃TƒCƒYAŒ`A‰^“®‚̉ðÍj–Ø‘º Šw
–ƒ¶ ®•¶Intraplate Deep Low Frequency Earthquakes far from Active Volcanoes iŠˆ‰ÎŽR‚©‚ç—£‚ꂽƒvƒŒ[ƒg“à‚Ì[•”’áŽü”g’nkjˆäo “N
‚“c Œ[l’á–§“xSiO2 Œ‹»‚̃wƒŠƒEƒ€’†‚ł̈³k‹““®‘DŽç “W³
’·’Jì ŒcSeismic Waveform Evidence for Existence of an Ultra-low Velocity Zone with Significant Amounts of Iron in the lowermost mantle beneath the central Pacific (’nk”gŒ`•ªÍ‚©‚玦´‚³‚ê‚é’†‰›‘¾•½—m‰ºƒ}ƒ“ƒgƒ‹Å‰º•”‚É‚¨‚¯‚é’´’ᑬ“x—̈æ‚Ì‘¶Ý)ƒQƒ‰[ ƒƒo[ƒg
”ä–¼ ËŽqDehydration and deformation processes of siliceous sediments in subduction zonesi’¾‚Ýž‚Ý‘Ñ‚É‚¨‚¯‚éŒ]Ž¿‘ÍÏ•¨‚Ì’E…E•ÏŒ`‰ß’öj–Ø‘º Šw
Žá—Ñ ‘å—C‚–§“x‰»SiO2 ƒKƒ‰ƒX‚̈³k‹““®‘DŽç “W³

•½¬23”N3ŒŽC—¹i•½¬22”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
”Ñ“c ˜a–çChronology, Petrology and Numerical Simulation for Cretaceous to Paleogene Granitic Rocks, SW Japan i¼“ì“ú–{”’ˆŸ‹I]ŒÃ‘æŽO‹I‰Ô›¼Šâ—Þ‚Ì”N‘ãŠw“IEŠâΊw“IŒ¤‹†‚¨‚æ‚Ñ”’lŒvŽZjŠâX Œõ
”’à_ ‹g‹NALOS ‰æ‘œ‚ð—p‚¢‚½Kumukol Basin ‚Ì•Ï“®’nŒ`‰ð͂ƃ`ƒxƒbƒg‚Œ´–k‰‚ÌŠg‘僃JƒjƒYƒ€‚ÌŒŸ“¢’r“c ˆÀ—²

•½¬22”N3ŒŽC—¹i•½¬21”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
“c‘º T‘¾˜NEffects of Material Heterogeneity on Branching Faults in a Subduction System i’¾‚Ýž‚Ý‘Ñ‚Ì•ªŠò’f‘w‚ɑ΂·‚é”}Ž¿•s‹ÏŽ¿‚̉e‹¿jˆäo “N

•½¬21”N3ŒŽC—¹i•½¬20”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‘¾“c ˜aWPrecise hypocenter distribution of deep low-frequency earthquakes and its relationship to the local geometry of the subducting plate in Nankai subduction zone, Japan (“ìŠCƒgƒ‰ƒt’¾‚Ýž‚Ý‘Ñ‚É‚¨‚¯‚é[•”’áŽü”g’nk‚̸–§kŒ¹•ª•z‚Æ‹ÇŠ“I‚ȃvƒŒ[ƒg\‘¢‚Æ‚ÌŠÖŒW)ˆäo “N
“í“c ç•äGeochemical and numerical studies on slab-derived fluids and the Arima-type brine (ƒXƒ‰ƒu‹NŒ¹—¬‘Ì‚Æ—L”nŒ^‰–…‚ÉŠÖ‚·‚é’n‹…‰»Šw ‚¨‚æ‚Ñ”’lƒ‚ƒfƒŠƒ“ƒOŒ¤‹†)ŠâX Œõ
¬¼ Œ’‰îShear velocity structure in the lowermost mantle beneath the western Pacific from waveform inversion i”gŒ`ƒCƒ“ƒo[ƒWƒ‡ƒ“‚É‚æ‚鼑¾•½—m‰º‚Ìʼnº•”ƒ}ƒ“ƒg ƒ‹S ”g‘¬“x\‘¢„’èjƒQƒ‰[ ƒƒo[ƒg
¬—Ñ ¡“úŽqDiagenesis, dehydration and deformation of pelagic sediments in ancient subduction zone inferred from bedded chert in the Inuyama area, Mino Belt i’¾‚Ý ž‚Ý‘Ñ‚É‚¨‚¯‚éƒ`ƒƒ[ƒg‘w‚Ì‘±¬E’E…‚Æ•ÏŒ`‚ÌŠÖŒW-”ü”Z‘ÑŒ¢ŽR’nˆæ‚æ‚è-j–Ø‘º Šw
–ì’à ‘¾ˆêParticle Analysis and Energetics of Fault Rocks: An Example from the Toyamagawa Fault, Central Japan i’·–쌧‰“ŽRì’f‘w‚ð—á‚Æ‚µ‚½C’f‘wŠâ‚Ì—±Žq‰ðÍ‹y‚уGƒlƒ‹ƒM[˜_j“c’† GŽÀ

•½¬20”N3ŒŽC—¹i•½¬19”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‰iˆä GŒ›Experimental Study of Pressure Effects on Microstructure of Partially-Molten Forsterite-Jadeite System i•”•ª—n—ZƒtƒHƒ‹ƒXƒeƒ‰ƒCƒg[ƒqƒXƒC‹PÎŒn‚Ì”÷×\‘¢‚ւ̈³—ÍŒø‰Ê‚ÌŽÀŒ±“IŒ¤‹†j¬àV ˆêm
㞊 —T‹v’PŽÎ‹P΃|[ƒtƒBƒƒNƒ‰ƒXƒg‚ð—p‚¢‚½ƒ}ƒ“ƒgƒ‹‚©‚ñ‚ç‚ñŠâ‚̉·“x-ˆ³—Í-•ÏŒ`Žw•W `–y–ž‚©‚ñ‚ç‚ñŠâ‘Ì‚Ì㸗š—ð‚Ö‚Ì“K‰ž¬àV ˆêm
‘—t —zŽqShear zone growth on the splay fault in accretionary prism |the footwall of the Nobeoka Thrust in the Shimanto Belt (‹ãBŽl–œ\‘щ„‰ªÕã’f‘w‚©‚猩‚éout-of-sequence- thrust‚Ì™’’f‘Ñ‚Ì”­’B)–Ø‘º Šw
œAì ’q—²Õ’Ãì’f‘w‚É‚¨‚¯‚é, ”÷¬’nk‘½”­/‹ó”’—̈æ‚Ì’f‘wŠâ”äŠrŒ¤‹†“c’† GŽÀ
–kžŠ ˆ¤Deformation and diagenesis of sandstones in underthrusted sediments -An example from the Mugi Melange, Shikoku, Japan- i•t‰Á‘Ì’†‚Ì‘ÍÏ•¨‚ªŽó‚¯‚鑱¬‚¨‚æ‚Ñ•ÏŒ`‰ß’ö-Žl–œ\‘Ñ–´Šòƒƒ‰ƒ“ƒWƒ…‚Ì—á-j–Ø‘º Šw
¼”ö r•Fƒ_ƒCƒ„ƒ‚ƒ“ƒhƒAƒ“ƒrƒ‹‘•’u—pc-BNƒKƒXƒPƒbƒgŠJ”­‚Æ‚»‚̉ž—p‘DŽç “W³

•½¬19”N3ŒŽC—¹i•½¬18”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
²X–Ø •Ï¬Šâ’†‚ÉŒ»‚ê‚éå÷‹È\‘¢‚ÌŒ`¬‰ß’öŠâX Œõ
‰ª–{ L–çSlip mechanisms of a major out-of-sequence thrust in an accretionary complex ]Approaching from the Nobeoka Thrust in the Shimanto Belt, Kyushu Japan]–Ø‘º Šw
ꎓ¡ —F”äŒÃÕ’Ãì’f‘w”jÓ‘Ñ‚Ì’f‘wŠâƒRƒA‚ð—p‚¢‚½’nŠkƒKƒX¶¬^•úoŽÀŒ±“c’† GŽÀ
‚‹´ ˆŸ—[Young lava field on the old Pacific Plate just before its subduction: Volcanism induced by lithospheric flexureŠâX Œõ
•Ÿ‘º GŽ¡A model combining the Earth's thermal evolution and material fractionationŠâX Œõ
•yŽm ‰„Í1-D SH velocity models for the subregions of the Northwestern Pacific obtained using waveform inversionƒQƒ‰[ ƒƒo[ƒg

•½¬18”N3ŒŽC—¹i•½¬17”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
ã–Ø Œ«‘¾Subduction zone magmatism and mantle wedge structure of the Sengan region, Northeastern JapanŠâX Œõ
“ào ’•FDevelopment of Multiscale Slip Inversion Method and Its Application to the 2004 Mid-Niigata Prefecture Earthquakeˆäo “N
‰Y“c ‹IŽqƒ_ƒCƒŒ[ƒ^ƒ“ƒV[‚ðl—¶‚µ‚½thermal pressurization ƒ‚ƒfƒ‹‚Ì’nk’f‘w‚Ö‚Ì“K—p-–쓇’f‘wAŽÔâÄš¼’f‘w‚ð—á‚É‚µ‚Ä-“c’† GŽÀ
¬“c WˆÉ“ß’J’f‘w‘Ñ‚Ì\‘¢‚Æ‚»‚Ì”­’B‰ß’ö’r“c ˆÀ—²
¬“c“‡ —f_Cr-Al spinel as a deformation indicator for the upper mantle: observational study in the Horoman Peridotite Complex¬àV ˆêm
²“¡ —FŽq’´‚ˆ³‰º‚É‚¨‚¯‚é“ñŽ_‰»•¨‚Ìpost-PbCl2 ‘Š“]ˆÚ‚ÌŒ¤‹†‘DŽç “W³
–ì“c Žé”üInversion Analysis of Geodetic Data in the Kanto Region, Central Japan, with a 3-D Plate Interface Model: Diversity of Stress Release Modes¼‰Y [G
ŽRŒû ”ò’¹The origin of syntectonic veins in accretionary complex and its implication for fluid behavior around the up-dip limit of seismogenic zone–Ø‘º Šw

•½¬17”N3ŒŽC—¹i•½¬16”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‰ª“c ^‰îƒXƒ“ƒ_ŠCa—¤‘¤ŽÎ–Ê‚ÌŠC’ê•Ï“®’nŒ`‚Æ‚»‚Ì”­’B‰ß’ö’r“c ˆÀ—²
òŽR “O–ç"Mechanism of mantle upwelling and melting in
back arc region: constraints from the temporal and spatial variation of the 'plateau basalt' in northwestern Kyushu"
¬àV ˆêm
–x“à r‰î"Numerical study of melting in subduction zones
with variable viscosity"
ŠâX Œõ

•½¬16”N3ŒŽC—¹i•½¬15”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‘å•£ ’qŸƒvƒŒ[ƒg‹«ŠE‚É‚¨‚¯‚é’nk”­¶—lŽ®‚Ì‘½—l«‚ÉŠÖ‚·‚錤‹†¼‰Y [G
²“¡ ŠˆŽuA normal-faulting paleostress around the up-dip limit of seismogenic zone: An improvement of stress inversion method and its application to an onland accretionary complex–Ø‘º Šw
‹ß“¡ ‰pŽ÷Deformation and fluid flow through micro-cracks recorded in the Nobeoka thrust in the Shimanto Belt, Kyushu, Japan–Ø‘º Šw
Ž­‘q —m‰îNumerical Simulation for Geomorphic Evolution in Taiwan with a Stream Erosion Model¼‰Y [G

•½¬15”N3ŒŽC—¹i•½¬14”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‰¬’à ’BMechanisms of crustal differentiation of basaltic magmas: Constraints from the contrasting variation trends observed in Aogashima and@other Izu Arc volcanoes Œº•ŠâŽ¿ƒ}ƒOƒ}‚Ì’nŠk“à•ª‰»ƒƒJƒjƒYƒ€Fƒ–“‡‚¨‚æ‚шɓ¤ŒÊ‰ÎŽR‚É‚Ý‚ç‚ê‚é‘ÎÆ“I‚ȕω»ƒgƒŒƒ“ƒh‚©‚ç‚̧–ñ¬àV ˆêm
‰Í‡ Œ¤ŽuThe Direct Solution Method for computing synthetic seismograms in transversely isotropic spherically symmetric media and its applicationsƒQƒ‰[ ƒƒo[ƒg
ì’[ ŒP‘ãApllication of the isocon method to argillaceous rocks of accretionary complex and@quantitavive estimation of volume change due to mass transfer associated with deformation i•t‰Á‘Ì“DŽ¿Šâ‚Ö‚Ìisocon–@‚Ì“K—p‚Æ•ÏŒ`‚É”º‚¤Ž¿—ʈړ®‚É‚æ‚é‘Ìϕω»‚Ì’è—Ê“IŒ©Ï‚à‚èj–Ø‘º Šw
–k‘º —LvMagnetic fabric of underplated melange and its relationship with lithology of the@Shimanto Belt, southwest Japan i¼“ì“ú–{AŽl–œ\‘Ñ‚ÉŒ©‚é’ꂯƒƒ‰ƒ“ƒWƒ…‚ÌŽ¥«ƒtƒ@ƒuƒŠƒbƒN‚ÆŠâ‘Š‚Æ‚ÌŠÖŒWj–Ø‘º Šw
Ž›ì ŽõŽqƒTƒ“ƒAƒ“ƒhƒŒƒAƒXŒ^‰¡‚¸‚êƒvƒŒ[ƒg‹«ŠE‚Ìâ‘΋­“x„’載Y [G
’†‘º m”ü—¼”’ŽR’n‚É‚¨‚¯‚é’¾‚Ýž‚ݑщάŠˆ“®ŠâX Œõ
•Ÿˆä Œ’ŽjDevelopment of a 3D Standard Model of Plate Interfaces in and around Japan: Physical Interpretation of Long-term Crustal@Movements in Kanto District i“ú–{—ñ“‡ˆæ‚ÌŽOŽŸŒ³ƒvƒŒ[ƒg‹«ŠEŒ`󃂃fƒ‹‚Ì\’zFŠÖ“Œ’nˆæ‚Ì’·Šú“I’nŠk•ÏŒ`‰^ “®‚̉ð–¾j¼‰Y [G
¼‘º ³”VP-T condition and heterogeneous fluid flow through cracks in the underthrusted melange- observation from the Shimanto Belt, Japan i’¾‚Ýž‚ñ‚¾ƒƒ‰ƒ“ƒWƒ…‚É‚¨‚¯‚銄‚ê–Ú‚ð’Ê‚µ‚½•s‹ÏŽ¿‚È—¬‘Ì‚Ì—¬‚ê‚Ɖ·“xEˆ³—ÍðŒ[Žl–œ\‘Ñ ‚Å‚ÌŠÏŽ@j–Ø‘º Šw
ŽR–{ Žu”TXü‰ñÜ–@‚É‚æ‚éMgSiO3ƒƒ‹ƒg‚ÆCaSiO3ƒƒ‹ƒg‚Ì\‘¢‚̈³—͕ω»‚ÌŒ¤‹†‘DŽç “W³
DJURAEV OmonEfficient and accurate methods for evaluating analytic solutions of the elastic equation of motion and their application to data analysis i‚¸“x‹y‚Ñ‚ŒvŽZ”\—¦‚ð—L‚·‚é’e«‘̂̉^“®•û’öŽ®‚̉ðÍ“I‰ð‚«•û‚Æ‚»‚̉ž—pjƒQƒ‰[ ƒƒo[ƒg

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